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The greenstone belt and metamorphosed microclastic rock-type superlarge gold deposits in China are hosted in metamorphic rocks and later intrusive bodies.Sedimentation.regional metamorphism and mineralization contributed a lot to the formation of the deposits,so did remelting magmatic process to some deposits,but the deposits were finally formed by reworking processes.The key factor leading to the formation of superlarge gold deposits is the reworking intensity,which for superlarge gold deposits is reflected by the large-scale reworked source rocks and even ore materials of various sources,strongly oxidized ore-forming fluids with a long and repeated active history and stable geothermal heat current.The factor which decides the reworking intensity is the network consisting of structures of different classes. 相似文献
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大沟谷金矿床产于震旦系乐晶峡群钠长石岩带底部陡倾斜钠长石岩中。金矿床铅同位素组成变化大^206Pb/^204Pb17.356-19.306,^207Pb/^204Pb15.330-15.862,^208Pb/^204Pb37.532-39.957。u值在8.23-10.6之间,黄铁矿δ^34S值在5.1‰-13.4‰之间,铅同位素组成具线性相关关系,^206Pb/^204Pb与^207Pb/^204Pb线性方程y=0.24x 11.19,r=0.83,^206Pb/^204Pb与^208Pb/^204Pb方程为y=1.3x 14.8,r=0.93,黄铁矿铅硫同位素组成具负相关关系,钠长石岩Rb、Sr含量较低,^87Sr/^86Sr值为0.72263-0.73150,平均0.72595。综合铅、锶、硫同位素特征,可以认为大沟谷金矿床成矿物质主要来自高u值基底碎屑沉积岩及钠化基性火成岩。 相似文献
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Gold deposits in intrusive masses include the veinlet dissemination,quartz vein and veinlet dissemination vein types,They are distributed in fracture zones along the endocontact zone of a batholith or in the centre and edge of a stock.The metallogenic epochs are Yenshanian,Hercynian,Archean,Proterozoic and Himalayan,The gold deposits are characterized by a big difference in time span between gold mineralization and the formation of host masses Ore-forming materials were derived from the masses and auriferous strata and ore-forming fluids came from meteoric and formation waters.When circulating water was heated by ascending heat flow,gold would be extracted,concentrated and transported from auriferous rocks and then precipitated in the masses during the late tectonic movement,Finally gold deposits were formed in the intrusive masses. 相似文献
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花岗岩类岩体与金矿床成因关系的探讨 总被引:1,自引:0,他引:1
花岗岩类岩体与金矿床存在着密切的空间联系,其在罪状每直是矿床学界争率的焦点,上前诉岩浆热液成因观点仍居统治地位。随着地质资料的积累,高温高压实验技术,尤其是金矿床同位素定年技术的进展,传统观战受到了严峻挑战。 相似文献